相关实验视频
Updated: Jul 12, 2026

08:14
Atom Probe Tomography Analysis of Exsolved Mineral Phases
Published on: October 25, 2019
概括
在萨德伯里有不寻常的变形结构.
科学领域:
- 地质地质地质地质地质地
- 冲击石坑的形成
- 冲击变形的发生是因为冲击变形.
背景情况:
- 在安大略省萨德伯里的Onaping构造中,含有地下岩石包含.
- 这些隙中的变形结构类似于已知的撞击坑中发现的变形结构.
研究的目的:
- 为了调查奥纳平形成中不寻常的变形结构的起源.
- 为了确定这些结构是否表明石撞击.
主要方法:
- 石英平面变形特征的显微镜检查 (PDF).
- 观察到的结构与已知撞击地点的结构进行比较.
主要成果:
- 在石英中确定了平面集,并行于特定的晶体平面 (0001) 和 (10ī3).
- 这些特征是超高速冲击造成的冲击变形的特征.
结论:
- 观察到的变形结构强烈暗示了石撞击起源的Onaping形成.
- 形成可能由冲击和融化材料组成,这些材料在萨德伯里盆地冲击事件发生后不久沉积起来.
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